Pregled bibliografske jedinice broj: 10430
Ammonium Ion Bearing Hyalophane Feldspar, Busovača, Central Bosnia; Metamorphogenic Origin Constrained by CO2-Inclusion Study
Ammonium Ion Bearing Hyalophane Feldspar, Busovača, Central Bosnia; Metamorphogenic Origin Constrained by CO2-Inclusion Study // Abstracts. Abstract Supplement No 1. Terra Nova. Volume 9 / EUG Scientific Committee chairman A. Kroner (Mainz) (ur.).
Strasbourg: Cambridge University Press, 1997. (poster, nije recenziran, sažetak, znanstveni)
CROSBI ID: 10430 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Ammonium Ion Bearing Hyalophane Feldspar, Busovača, Central Bosnia; Metamorphogenic Origin Constrained by CO2-Inclusion Study
Autori
Palinkaš, Ladislav ; Bermanec, Vladimir ; Jurković, Ivan ; Zebec, Vladimir ; Pavlović, Gordana
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
Abstracts. Abstract Supplement No 1. Terra Nova. Volume 9
/ EUG Scientific Committee chairman A. Kroner (Mainz) - Strasbourg : Cambridge University Press, 1997
Skup
European Union of Geosciences. Biennal EUG 9 Meeting
Mjesto i datum
Strasbourg, Francuska, 23.03.1997. - 27.03.1997
Vrsta sudjelovanja
Poster
Vrsta recenzije
Nije recenziran
Ključne riječi
Alpine-type quartz-hyalophane veins; fluid inclusion study of quartz; nitrogen in hyalophane;Bosnia
Sažetak
Alpine-type quartz-hyalophae veins cut Lower Palaeozoic metasediments. Electron microprobe analyses determined 0.12% nitrogen in hyalophane and IR confirmed presence of ammonium ion. Fluid inclusion study of quartz gave: TFMCO2 60 to 37 C; TLMCO2 58 to 56.5 C; TLMIce -11.7 to -4 C; TLMCLATHRATE +2.5 to +6.2 C; THCO2 +14.6 to +29.2 C; ThTOT +300 to 322 C; salinity 6.6 to 13.5 wt% NaClequ.; FLS contain 0.55 to 8.80% , density 0.98 g/cm3, TMTOT 313 C, pressure 2.25 kbars. Fluids are of typical metamorphogenic origin.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb,
Rudarsko-geološko-naftni fakultet, Zagreb
